侏罗系冻结砂岩单轴抗压强度与孔隙度的关联性分析

    Correlation Analysis of Porosity and Uniaxial Compressive Strength of Jurassic Frozen Sandstone

    • 摘要: 为研究冻结条件下岩石的孔隙度与单轴抗压强度之间的关系,对人工冻结条件下的侏罗系饱和含水砂岩进行了核磁共振测试和单轴压缩试验;分析了不同温度条件下,温度与单轴抗压强度和孔隙度之间的关系,并将孔隙度和单轴抗压强度进行了关联分析。研究结果表明:砂岩单轴抗压强度和温度满足二次曲线变化关系;-5~-15 ℃等温度区间,单轴抗压强度增长值从4.54 MPa降至0.54 MPa,单轴抗压强度增长率从14.22%降至1.33%;饱和冻结砂岩孔隙度随着温度的下降,其孔隙度亦减小,且孔隙度和温度的关系符合幂指函数变化规律;冻结砂岩孔隙度和其单轴抗压强度满足幂指函数关系。

       

      Abstract: To study the relationship between rock porosity and uniaxial compressive strength under freezing conditions, NMR and uniaxial compression tests were performed on Jurassic saturated aquifer sandstone under artificial freezing conditions. The relationship between temperature and uniaxial compressive strength and porosity under different temperature conditions was analyzed, and the porosity and uniaxial compressive strength were correlated. The results show that: the uniaxial compressive strength and temperature of sandstone satisfy the quadratic curve relationship; from -5 ℃ to -15 ℃, the increase value in uniaxial compressive strength decreases from 4.54 MPa to 0.54 MPa. The axial compressive strength growth rate decreased from 14.22% to 1.33%; the porosity of saturated frozen sandstone decreases with temperature, and its porosity also decreases, and the relationship between porosity and temperature complies with the power index function; the porosity of frozen sandstone and its uniaxial compressive strength meet the power index function relationship.

       

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